Page 177 - Origin and Prediction of Abnormal Formation Pressures
P. 177

d

             152                       o c  dc  dr.
                                                 W.H. FERTL, G.V. CHILINGAR AND J.O. ROBERTSON JR.
                                                                              i
                                                                           I8't~
                                                                               n
                      0.9   d~                                            9
                     ,,C,.811,0   v  1;5  2.   1.   t.5   2.0   1.0   1.,5   2~0  2'   0 .81  1./0  ""  1.5   2.0  ,
                                                                         "
                                                                       Illll((lllli) \  .
                                                i      i          i
                     -
              g
              2                                     lO                      6~2 in.

              =2                          ,._   ...


                                                                           '
              a              g                      11
                                                                                  1
                                                                               _
                                                                                  '
                   10                                                 11111111~111
                      11,411111 o-    I                II
                          A                 B              C                D
             Fig.  6-1.  Plotting  the  dc-exponent  on  a  logarithmic  scale  using  the  mud  weight  overlay  technique  in  South
             Texas  (A,D),  South  Louisiana  (B)  and  Oklahoma  (C).  (After  Zamora,  1972,  fig.  2,  p.  70.  In  Chilingarian
             and  Vorabutr,  1981,  fig.  16-5,  p.  588.)  Note  effect  of bit  size  change  (from  8  1/2  inches  to  6 1/2  inches)  on
             normal  trendline  in  the  South  Texas  well  (D).  Trendlines  represent  constant  mud  specific  weights.  (Courtesy
             of Oil and Gas Journal.)

             lb), and rotary speed (N, in rpm):
                       log(R/6ON)
                 d-   log(12W/lO6D)                                              (6-1)

               Basically,  plots  of d-exponent  versus  depth  show  a  decreasing  trend  with  depth.  In
            transition  zones  and  overpressured  environments,  in  many  cases  the  calculated  values
            diverge  from  the  normal  trend  to  lower  than  normal  values.  Quantitative  pressure
            evaluation can then be made on using the equivalent depth method (Fertl,  1976, p.  123)
            or specially constructed,  transparent overlay of parallel, equivalent mud weight lines for
            the specific depth scale used for the d-exponent (see Fig. 6-1).
               The values of the d-exponent are affected by any change in the basic input parameters
            in Eq. 6-1. Furthermore,  it is often difficult to establish reasonable values for bit weight
            in soft formations.  Any major lithologic  change in the shale section (e.g., limey or silty
            shales, mudstones,  and marls) will also affect the d-exponent. The same is true in poorly
            maintained drilling fluid systems and for drastic changes in mud weight.
               Inasmuch  as  Eq.  6-1  ignores  the  direct  effect  of  mud  weight  on  drilling  rate,  a
            modification  of the  d-exponent  has  been  proposed  by  Harper  (1969)  to  normalize  the
            d-exponent for the effective mud weight as follows:
                        MW1
                 dc -- d.  MW2                                                  (6-2)
            where dc is modified  (corrected) d-exponent,  MW1  is normal  mud weight,  and MW2 is
            actual mud weight used.
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